DOCSLIB.ORG

The Dalton Highway

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
The Dalton Highway Te DaDallHtt ooi g nnh w a y Visitor Guide Road Conditions . pages 6-7 Points of Interest . .page 8 Bear Safety . .page 16 Contents Ultimate Road Adventure Trip Planning The Dalton Highway is a rough, industrial road that begins 84 miles/134 km north of Fairbanks and ends 414 miles/662 km later in 4 Preparing and Safety Deadhorse, the industrial camp at Prudhoe Bay. It provides a rare 6 Mileage Chart opportunity to traverse a remote, unpopulated part of Alaska to the 11-14 Maps very top of the continent. Traveling this farthest-north road involves real risks and challenges. This publication will help you decide 23 Planning Your Trip whether to make the journey, how to prepare, and how to enjoy your experience. Please read this information carefully. Exploring Know Before You Go 8-11 Points of Interest • There is no public access to the Arctic Ocean from Deadhorse. 15 An Icebound Land You must be on an authorized tour. Call toll-free 1-877-474-3565; 17 Watching Wildlife in Fairbanks, 474-3565. 18 Recreation • There are no medical facilities between Fairbanks and Deadhorse, a distance of 500 miles/800 km. For emergency information, see the back page. Facilities and Services • Food, gas, and vehicle repair service are extremely limited. 5 Visitor Centers See page 5. 18 Campgrounds • There is limited cell phone service and public Internet connection between Fairbanks and Deadhorse. The Dalton Highway BLM Coordinator: Kelly Egger Contributors: Eugene Ervine, Lenore Heppler, Lisa Shon Jodwalis, Craig McCaa, Pam Rice. John Rapphahn, Crystal Glassburn, Jason Oles, Jason Post Produced and Designed by All photos courtesy of the BLM unless otherwise noted. Arctic Interagency Visitor Center The award-winning Arctic Interagency Visitor Center introduces Printed on recycled paper using soy-based inks. visitors from around the world to the unique and extreme environment of the Arctic. Explore interpretive exhibits, walk the nearby nature The Dalton Highway Visitor Guide is trails, and talk with our knowledgeable staff to learn more about the published by the Alaska Geographic region’s history, natural environment, and recreation opportunities. Association in cooperation with the Bureau The visitor center is a partnership between the Bureau of Land of Land Management. This free publication is made possible by Alaska Geographic Management, the National Park Service, and the U.S. Fish and Wildlife bookstore sales. Service, and hosts an Alaska Geographic Association bookstore. ©Alaska Geographic Open Daily from May 24 to September 16, from 11 a.m. to 10 p.m. Phone: 907-678-5209 or 907-678-2014 (summer only). Cover photo: The Bettles River/Sukapak Mountain, MP 204. BLM photo by www.blm.gov/learn/interpretive-centers/aivc Carl Kretsinger Click on “Visitor Centers” and then on “Arctic Interagency Visitor Center” 2 Built for Black Gold In 1968, oil was discovered at Prudhoe Bay on Alaska’s North Slope. Excitement was high at the prospect of new money to fuel Alaska’s boom-and-bust economy. The nation was in the throes of an energy crisis and pushed for an 800-mile-long (1290 km) pipeline. But first, native land claims had to be settled, permits granted, environmental safeguards designed, and a road built to get workers and supplies north to the oil field. When finally approved, construction of the Trans- Alaska Pipeline was run like a wartime project— money was no object and time was of the essence. The weather conditions, terrain, and the immensity 2019 marks the 45th anniversary of the completion of the Haul Road, of the project were all extreme. Engineers overcame now known as the Dalton Highway. permafrost, mountain ranges, and the relentless flow of the Yukon River in the process. Incredibly, the The highway was open only to commercial traffic Haul Road was completed in just five months and until 1981, when the state allowed public access to the pipeline in three years (1974-77). The previously Disaster Creek at Milepost 211. In 1994, public access remote Arctic was changed forever. was allowed all the way to Deadhorse for the first time. Today, the Dalton Highway beckons adventurous souls Haul Road or Highway? to explore a still-wild and mysterious frontier. Respect At first, the highway was called the Haul Road because this harsh land and appreciate the opportunity to visit almost everything supporting oil development was a special part of our world. “hauled” on tractor-trailer rigs to its final destination. In 1981, the State of Alaska named the highway after James B. Dalton, a lifelong Alaskan and expert in arctic engineering who was involved in early oil exploration efforts on the North Slope. “....I trucked the Haul Road to Prudhoe a few hundred times and fshed Grayling Lake and hunted the South Fork Koyukuk for 10 years in a row. I really, really miss it—the beauty, quiet, and the freedom it brings one’s mind. It’s defnitely the best mental medicine on earth.” Marshall Casteel Myrtle Creek, Oregon 3 Weather Preparing for Summer temperatures can occasionally reach the high 80s F (27-30°C) south of the Brooks Range and average the Long Haul in the 50s F (10-15°C) in Coldfoot. Thunderstorms are common in early summer, especially between Before you leave Fairbanks Fairbanks and the Yukon River, and may bring • Inspect all tires and make sure they are properly inflated lightning and sudden squalls. In general, June and • Check all vehicle fluids July are drier months, but rainy days are frequent • Replace worn hoses and belts throughout the summer. • Empty your RV’s holding tank and fill the water tank Weather on the North Slope is frequently windy, • Purchase groceries and supplies foggy, and cold. Snow can occur at any time of the Bring for your vehicle year, especially from the Brooks Range north. In • At least two full-sized spare tires mounted on rims Deadhorse, average summer temperatures are in the • Tire jack and tools for flat tires 30s and 40s F (0-5°C). • Emergency flares • Extra gasoline, motor oil, and wiper fluid Flash Floods • CB radio Heavy or prolonged rain can cause local flash floods anytime during the summer. Running water may cover Bring for yourself the road or wash out culverts and bridges. Do not • Insect repellent and head net attempt to cross flooded areas. • Sunglasses and sunscreen • Rain jacket and pants Wildfires • Warm clothes, including hat and gloves Wildfires may burn out of control and across the • First aid kit highway. Do not drive through areas of dense smoke • Drinking water or flames—you could get trapped by swiftly changing • Ready-to-eat food conditions and find yourself unable to reach safety. • Camping gear, including sleeping bag • Personal medications Wildlife • Toilet paper and hand sanitizer Treat all wild animals with caution. Keep a clean • Garbage bags camp so you don’t attract wildlife. Do not approach or feed any animals. Moose and muskoxen may appear tame, but can be dangerous if approached too closely. Safety Tips Never get between a cow and her calves. If moose feel threatened they will flatten their ears, raise the hair Phones and Internet on their neck, and may charge. Wolves and foxes on • There is limited cell phone coverage and public Internet the North Slope may carry rabies. Avoid all contact access between Fairbanks and Deadhorse. Both are between these animals and yourself and your pets. available in Deadhorse. Coldfoot Camp and Yukon Crossing See page 17 for more information on where to look for have wi-fi (fee). wildlife. • Pay phones: You can use a calling card at the Yukon River Camp, Coldfoot, Wiseman, and Deadhorse. • Satellite phones: Some companies in Fairbanks rent satellite phones; check the phone directory under radio. Drinking Water • It’s best to bring water with you. If you must use stream water for cooking or cleaning, treat it first by boiling rapidly for 3-5 minutes, or by using iodine tablets or a water filter. Giardia is widespread in Alaska waters and is highly contagious. Fireweed abounds due to recent fre activity near the pipeline. 4 Visitor Information Centers In Fairbanks Morris Thompson Center Alaska Public Lands Information Center 101 Dunkel Street, #110 Fairbanks, AK 99701 Phone: 907-459-3730 Fax: 907-459-3729 [email protected] Open: year-round Services Are Limited At the Yukon River Notice: There are no public services at Department of Transportation Yukon Crossing Visitor maintenance stations or Alyeska Pipeline Service Company pump stations. Contact Station/AKGeo book store located on the Medical Facilities: There are no public or emergency medical facilities along east side of the highway just the Elliott or Dalton highways. north of the Yukon River Banking: There are no banks. ATM machines are available in Deadhorse. Most bridge. No phone. Closed in services accept major credit cards and traveler’s checks. winter. Yukon River camp is open year-round. Groceries: There are no grocery stores along the highway. Snack food and cafés are available at several locations. In Coldfoot Phone: There is limited cell phone coverage from Elliott Highway Milepost 28 Arctic Interagency until just outside of Deadhorse. Wi-fi available for a fee at Coldfoot Camp and Visitor Center Yukon Crossing. Coldfoot, MP 175 ss s ss Phone: 907-678-5209 SERVICES Yukon Crossing Five Mile Coldfoot Wiseman Deadhorse (summer only). Open daily Gas D D D from May 24–September 16. Tire/Vehicle Repair D D Closed in winter. Restaurant D D D D Lodging D D D D D Public Phone D D D D Post Ofce D D Shower D D D D Water D D D Laundry D D Dump Station D Tent Camping D D RV Parking D D Gift Shop/Local Crafts D D D D D Visitor Center/Museum D D D s closed in winter ss limited services in winter 5 Road Conditions Rules of the Road The road is narrow, has soft shoulders, high D Big trucks have the right of way.
Load more

Recommended publications
  • Northern Sea Route Cargo Flows and Infrastructure- Present State And
    Northern Sea Route Cargo Flows and Infrastructure – Present State and Future Potential By Claes Lykke Ragner FNI Report 13/2000 FRIDTJOF NANSENS INSTITUTT THE FRIDTJOF NANSEN INSTITUTE Tittel/Title Sider/Pages Northern Sea Route Cargo Flows and Infrastructure – Present 124 State and Future Potential Publikasjonstype/Publication Type Nummer/Number FNI Report 13/2000 Forfatter(e)/Author(s) ISBN Claes Lykke Ragner 82-7613-400-9 Program/Programme ISSN 0801-2431 Prosjekt/Project Sammendrag/Abstract The report assesses the Northern Sea Route’s commercial potential and economic importance, both as a transit route between Europe and Asia, and as an export route for oil, gas and other natural resources in the Russian Arctic. First, it conducts a survey of past and present Northern Sea Route (NSR) cargo flows. Then follow discussions of the route’s commercial potential as a transit route, as well as of its economic importance and relevance for each of the Russian Arctic regions. These discussions are summarized by estimates of what types and volumes of NSR cargoes that can realistically be expected in the period 2000-2015. This is then followed by a survey of the status quo of the NSR infrastructure (above all the ice-breakers, ice-class cargo vessels and ports), with estimates of its future capacity. Based on the estimated future NSR cargo potential, future NSR infrastructure requirements are calculated and compared with the estimated capacity in order to identify the main, future infrastructure bottlenecks for NSR operations. The information presented in the report is mainly compiled from data and research results that were published through the International Northern Sea Route Programme (INSROP) 1993-99, but considerable updates have been made using recent information, statistics and analyses from various sources.
    [Show full text]
  • QUICK REFERENCE GUIDE Latitude, Longitude and Associated Metadata
    QUICK REFERENCE GUIDE Latitude, Longitude and Associated Metadata The Property Profile Form (PPF) requests the property name, address, city, state and zip. From these address fields, ACRES interfaces with Google Maps and extracts the latitude and longitude (lat/long) for the property location. ACRES sets the remaining property geographic information to default values. The data (known collectively as “metadata”) are required by EPA Data Standards. Should an ACRES user need to be update the metadata, the Edit Fields link on the PPF provides the ability to change the information. Before the metadata were populated by ACRES, the data were entered manually. There may still be the need to do so, for example some properties do not have a specific street address (e.g. a rural property located on a state highway) or an ACRES user may have an exact lat/long that is to be used. This Quick Reference Guide covers how to find latitude and longitude, define the metadata, fill out the associated fields in a Property Work Package, and convert latitude and longitude to decimal degree format. This explains how the metadata were determined prior to September 2011 (when the Google Maps interface was added to ACRES). Definitions Below are definitions of the six data elements for latitude and longitude data that are collected in a Property Work Package. The definitions below are based on text from the EPA Data Standard. Latitude: Is the measure of the angular distance on a meridian north or south of the equator. Latitudinal lines run horizontal around the earth in parallel concentric lines from the equator to each of the poles.
    [Show full text]
  • Taltheilei Houses, Lithics, and Mobility
    University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2012-09-06 Taltheilei houses, lithics, and mobility Pickering, Sean Joseph Pickering, S. J. (2012). Taltheilei houses, lithics, and mobility (Unpublished master's thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/27975 http://hdl.handle.net/11023/177 master thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY Taltheilei Houses, Lithics, and Mobility by Sean J. Pickering A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS DEPARTMENT OF ARCHAEOLOGY CALGARY, ALBERTA SEPTEMBER, 2012 © Sean J. Pickering 2012 Abstract The precontact subsistence-settlement strategy of Taltheilei tradition groups has been interpreted by past researchers as representing a high residential mobility forager system characterized by ephemeral warm season use of the Barrenlands environment, while hunting barrenground caribou. However, the excavation of four semi-subterranean house pits at the Ikirahak site (JjKs-7), in the Southern Kivalliq District of Nunavut, has challenged these assumptions. An analysis of the domestic architecture, as well as the morphological and spatial attributes of the excavated lithic artifacts, has shown that some Taltheilei groups inhabited the Barrenlands environment during the cold season for extended periods of time likely subsisting on stored resources.
    [Show full text]
  • AIM: Latitude and Longitude
    AIM: Latitude and Longitude Latitude lines run east/west but they measure north or south of the equator (0°) splitting the earth into the Northern Hemisphere and Southern Hemisphere. Latitude North Pole 90 80 Lines of 70 60 latitude are 50 numbered 40 30 from 0° at 20 Lines of [ 10 the equator latitude are 10 to 90° N.L. 20 numbered 30 at the North from 0° at 40 Pole. 50 the equator ] 60 to 90° S.L. 70 80 at the 90 South Pole. South Pole Latitude The North Pole is at 90° N 40° N is the 40° The equator is at 0° line of latitude north of the latitude. It is neither equator. north nor south. It is at the center 40° S is the 40° between line of latitude north and The South Pole is at 90° S south of the south. equator. Longitude Lines of longitude begin at the Prime Meridian. 60° W is the 60° E is the 60° line of 60° line of longitude west longitude of the Prime east of the W E Prime Meridian. Meridian. The Prime Meridian is located at 0°. It is neither east or west 180° N Longitude West Longitude West East Longitude North Pole W E PRIME MERIDIAN S Lines of longitude are numbered east from the Prime Meridian to the 180° line and west from the Prime Meridian to the 180° line. Prime Meridian The Prime Meridian (0°) and the 180° line split the earth into the Western Hemisphere and Eastern Hemisphere. Prime Meridian Western Eastern Hemisphere Hemisphere Places located east of the Prime Meridian have an east longitude (E) address.
    [Show full text]
  • A Trip to Alaska's Brooks Range Is the Trip of a Lifetime. You’Ll See Herds of Caribou Migrating Like They Have for Thousands of Years
    Hunt ID: AK-GBearMooseCaribou-Rifle-Kotzebue-AKO-Wayne A trip to Alaska's Brooks Range is the trip of a lifetime. You’ll see herds of caribou migrating like they have for thousands of years. If you feel comfortable you can take an outfitted semi-guided Caribou Hunt for the largest member of the caribou family, the barren ground caribou. Grizzly bear are often seen splashing after salmon in the river or foraging for berries on the tundra. Moose and other wildlife, including black bears, wolverine, and wolves are seen not far from camp often. He has been hunting in this area for over 40 years and guiding for over 20 years. His son’s adult sons assist with running the camp and guiding. They have both grown up hunting in the area and pride themselves with providing you a hunt of a life time. The enormous size of the big game animals has much to do with their location so far north they must have hung bulk to withstand the long cold winter. The camp is located above the Arctic Circle, in the Squirrel River Valley of the western Brooks Range. Clients fly into the Inupiaq village of Kotzebue where they board small bush planes for the 80 mile trip to the hunting area. Base camps consist of comfortable free standing Hansen Weatherport tents with cots and heaters, including a shower tent. The main tent is a cooking area and gathering point for discussing the days hunt. Cooking is provided by the staff using a modern 4 burner gas stove with oven.
    [Show full text]
  • Mapping Traditional Place Names Along the Koyukuk River—Koyukuk
    Mapping Traditional Place Names along the Koyukuk River— Koyukuk, Huslia, and Hughes, Western Interior Alaska Introduction Koyukon Athabascan peoples have settled along the Koyukuk River in Western Interior Alaska for thousands of years using the surrounding landscape for subsistence and cultural resources. However, recent changes in climate, technology, resource availability, and way of life have affected land-use patterns in the region, as well as use of the Denaakk'e (Koyukon) language. The current Koyukon population is about 2,300, and about 150 still speak the language (the youngest of whom are in their fifties). In addition, Elders, important keepers of both language and traditional subsistence-use areas, are aging, and opportunities to record their knowledge are diminishing. “If place names are left undocumented then the owners and history of those places remain invisible. Place names provide clear evidence of land use and demonstrate Native presence in an area” Study area map representing the 366 spatially verified place names along the Koyukuk River from Koyukuk to Hughes. Gary Holton, Director of the Alaska Native Language Archive, Alaska Native Language Center Project Goals The goals of the place names project are to collect, preserve, cultivate, and pass on the rich knowledge and culture of the Koyukon people with regards to traditional place names and subsistence-use areas along the Koyukuk River in the villages of Koyukuk, Huslia, and Hughes. Place names provide important information regarding navigation, resource availability, cultural history, land ownership, and changes in land use. Archiving information of this nature assists in passing local and traditional knowledge to subsequent generations.
    [Show full text]
  • Why Do We Use Latitude and Longitude? What Is the Equator?
    Where in the World? This lesson teaches the concepts of latitude and longitude with relation to the globe. Grades: 4, 5, 6 Disciplines: Geography, Math Before starting the activity, make sure each student has access to a globe or a world map that contains latitude and longitude lines. Why Do We Use Latitude and Longitude? The Earth is divided into degrees of longitude and latitude which helps us measure location and time using a single standard. When used together, longitude and latitude define a specific location through geographical coordinates. These coordinates are what the Global Position System or GPS uses to provide an accurate locational relay. Longitude and latitude lines measure the distance from the Earth's Equator or central axis - running east to west - and the Prime Meridian in Greenwich, England - running north to south. What Is the Equator? The Equator is an imaginary line that runs around the center of the Earth from east to west. It is perpindicular to the Prime Meridan, the 0 degree line running from north to south that passes through Greenwich, England. There are equal distances from the Equator to the north pole, and also from the Equator to the south pole. The line uniformly divides the northern and southern hemispheres of the planet. Because of how the sun is situated above the Equator - it is primarily overhead - locations close to the Equator generally have high temperatures year round. In addition, they experience close to 12 hours of sunlight a day. Then, during the Autumn and Spring Equinoxes the sun is exactly overhead which results in 12-hour days and 12-hour nights.
    [Show full text]
  • Historic Land Use Processes in Alaska's Koyukuk River Area
    ARCTIC VOL. 42. NO. 2 (JUNE 1989) P. 148-162 Historic Land Use Processes in Alaska’s Koyukuk River Area WENDY H. ARUNDALE‘ and ELIZA JONES’ (Received 9 February 1988; accepted in revised form 21 September 1988) ABSTRACT. Northern Athabaskans with extensive knowledge of their traditional history and culture are increasingly interested in preserving their heritage. The authors areworking with Allakaket area Koyukon people in Alaska to record data on importanthistoric sites and events, but they are also using ethnoarchaeological approaches, particularly Binford’s models of settlement systems and site mobility, to help make the information they gather more valuable to both local Native people and archaeologists. Drawing on their preliminary data, as well as existing research, they describe changes in the late winter part of the seasonal round, showing how, over time, the Koyukon become more logistically organized as they become more sedentary. These changes have interesting archaeological implications, including effects on site mobility patterns. The Koyukon belief system, withan intricate set of traditional beliefs and practices, has significant, though largely unexplored potential for influencing archaeological variability. Key words: Alaska, Athabaskans, archaeology, belief systems, boreal forest, ethnoarchaeology, historic archaeology, historic sites, Koyukon, Koyukuk River, landscape use, settlement patterns, Subarctic RÉSUMÉ. Les Athabaskans du Nord qui possèdent une connaissance approfondie de leur histoire et de leur culture traditionnelles, sont de plus en plus intéressés à préserver leur patrimoine. Les auteurs travaillent actuellement avec des gens de la tribu Koyukon de la région d’Allakaket en Alaska, à consigner des données sur d’importants sites et événements historiques, mais ils utilisent aussi des approches ethnoarchéologiques, en particulier les modèles de Binford se rapportant aux systèmes de peuplement et de migration d’un site à l’autre, pour rendre l’information recueille plus utile, àla fois à la population autochtoneet aux archéologues.
    [Show full text]
  • The Mesa Site: Paleoindians Above the Arctic Circle
    U. S. Department of the Interior BLM-Alaska Open File Report 86 Bureau of Land Management BLM/AK/ST-03/001+8100+020 April 2003 Alaska State Office 222 West 7th Avenue Anchorage Alaska 99513 The Mesa Site: Paleoindians above the Arctic Circle Michael Kunz, Michael Bever, Constance Adkins Cover Photo View of Mesa from west with Iteriak Creek in foreground. Photo: Dan Gullickson Disclaimer The mention of trade names or commercial products in this report does not constitute endorsement or recommendation for use by the federal government. Authors Michael Kunz is an Archaeologist, Bureau of Land Management (BLM), Northern Field Office, 1150 University Avenue, Fairbanks, Alaska 99709. Michael Bever is a project supervisor for Pacific Legacy Inc., 3081 Alhambra Drive, Suite 208, Cameron Park, CA 95682. Constance Adkins is an Archaeologist, Bureau of Land Management (BLM), Northern Field Office, 1150 University Avenue, Fairbanks, Alaska 99709. Open File Reports Open File Reports issued by the Bureau of Land Management-Alaska present the results of invento- ries or other investigations on a variety of scientific and technical subjects that are made available to the public outside the formal BLM-Alaska technical publication series. These reports can include preliminary or incomplete data and are not published and distributed in quantity. The reports are available while supplies last from BLM External Affairs, 222 West 7th Avenue #13, Anchorage, Alaska 99513 and from the Juneau Minerals Information Center, 100 Savikko Road, Mayflower Island, Douglas, AK 99824, (907) 364-1553. Copies are also available for inspection at the Alaska Resource Library and Information Service (Anchorage), the USDI Resources Library in Washington, D.
    [Show full text]
  • Icing Mound on Sadlerochit River, Alaska
    Short Papers and Notes ICING MOUND ON SADLERO- Sadlerochithas emerged from the CHIT RIVER, ALASKA* mountains, has arelatively low gra- dient and flows in a broad, braided bed Icing mounds- small to large domes, characterized by manyanastomosing mounds,and ridges resulting from an shallowchannels separated by bare, upwardarching of soiland ice asso- gravelly and bouldery bars (Fig. 2). AS ciated with fields of aufeis - have been is characteristic of all riversof the Arc- described in detailfor Siberia1. Icing tic Slope, the change from a single deep mounds have also been mentioned brief- channel to a braided pattern of many ly inconnection with aufeisfields in shallow channels allows the formation Alaskaby Leffigwell (ref. 2, p. 158) of an aufeis field every year near the and Taber (ref. 3, p. 1528; ref. 4, p. 249), mountain front. During the fall the but there is little descriptive literature shallow channels freeze early and the on this phenomenon in theNorth Amer- obstruction of the resulting ice causes ican Arctic. One such icing mound was the river to overflow its bars;this over- examined briefly by the author on June flow then freezes and by repeated freez- 25,1959 during the course of a trip down ing,overflow and freezingsuccessive the SadlerochitRiver in northeastern layers of ice are built up toform an Alaska (Fig. 1). aufeis field. Another factor contributing Fig. 1. Locationmap, Arctic Slope, Alaska. The SadlerochitRiver rises in the to the formation of large aufeis fields is Franklin Mountains of the eastern a source of water that persists for some Brooks Range and flows northwardin a time after freezingbegins.
    [Show full text]
  • New Late Carboniferous Heritschioidinae (Rugosa) from the Kuiu Island Area and Brooks Range, Alaska
    Geologica Acta, Vol.12, Nº 1, March 2014, 29-52 DOI: 10.1344/105.000002074 New Late Carboniferous Heritschioidinae (Rugosa) from the Kuiu Island area and Brooks Range, Alaska J. FEDOROWSKI1 C.H. STEVENS2 E. KATVALA3 1Institute of Geology, Adam Mickiewicz University Makow Polnych 16, PL-61-606, Poznan, Poland. E-mail: [email protected] 2Department of Geology, San Jose Unversity San Jose, California 95192, USA. E-mail: [email protected] 3Department of Geology, University of Calgary Calgary, Canada. E-mail: [email protected] ABS TRACT Three new species of the genus Heritschioides, i.e., H. alaskensis sp. nov., H. kuiuensis sp. nov., and H. splendidus sp. nov., and Kekuphyllum sandoense gen. et sp. nov. from the northeastern Kuiu Island area and nearby islets, part of Alexander terrane in southeastern Alaska, and Heritschioides separatus sp. nov. from the Brooks Range, Alaska, are described and illustrated. The three new fasciculate colonial coral species from the Kuiu Island area, collected from the Moscovian Saginaw Bay Formation, are phylogenetically related to those of probable Bashkirian age in the Brooks Range in northern Alaska as shown by the presence of morphologically similar species of Heritschioides. These corals from both areas also are related to one species in the Quesnel terrane in western Canada. Kekuphyllum sandoense from the Saginaw Bay Formation of the Kuiu Island area is the only cerioid-aphroid species within the Subfamily Heritschioidinae described so far. The complete early ontogeny of a protocorallite is for the first time described here on a basis of H. kuiuensis sp. nov. and compared to the hystero-ontogeny in order to show similarities and differences in those processes.
    [Show full text]
  • Fort Yukon Hunting / Unit 25
    Fort Yukon Hunting / Unit 25 $UFWLF9LOODJH &KDQGDODU :LVHPDQ &KULVWLDQ &ROGIRRW 9HQHWLH &KDON\LWVLN )RUW<XNRQ %HDYHU %LUFK&UHHN 6WHYHQV9LOODJH )RUW+DPOLQ &LUFOH &HQWUDO 5DPSDUW /LYHQJRRG &LUFOH+RW6SULQJV (XUHND 0LQWR )R[ &KHQD )$,5%$1.6 +RW (DJOH 6SULQJV Federal Public Lands Open to Subsistence Use 2014/2016 Federal Subsistence Wildlife Regulations 115 Unit 25 / Hunting (See Unit 25 Fort Yukon map) Unit 25 consists of the Yukon River drainage upstream from (but excluding) the Hamlin Creek drainage; and excluding drainages into the south bank of the Yukon River upstream from the Charley River. Unit 25A consists of the Hodzana River drainage rivers; and drainages into the north bank of the Yukon River upstream from the Narrows; the Chandalar River drainage upstream from Circle, including the islands in the Yukon upstream from (and including) the East Fork drainage; River. the Christian River drainage upstream from Christian; the Unit 25C consists of drainages into the south bank of Sheenjek River drainage upstream from (and including) the the Yukon River upstream from Circle to the Unit 20E Thluichohnjik Creek; the Coleen River drainage; and the boundary; the Birch Creek drainage upstream from the Old Crow River drainage. Steese Highway bridge (milepost 147); the Preacher Creek Unit 25B consists of the Little Black River drainage drainage upstream from (and including) the Rock Creek upstream from (but excluding) the Big Creek drainage; drainage; and the Beaver Creek drainage upstream from the Black River drainage upstream from (and including) (and including) the Moose Creek drainage. the Salmon Fork drainage; the Porcupine River drainage Unit 25D consists of the remainder of Unit 25.
    [Show full text]